limestone and marble
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Limestone and marble are two types of rocks that can be easily weathered by carbonic acid. This is because carbonic acid reacts with the calcium carbonate in these rocks, leading to the formation of calcium bicarbonate and ultimately causing dissolution and erosion of the rock.
Limestone and marble are two types of rocks that are easily weathered by carbonic acid due to their high calcium carbonate content. Over time, carbonic acid dissolves these rocks, leading to the formation of caves, sinkholes, and other karst landscapes.
H2CO3 is carbonic acid. Carbonic acid is a weak acid that is excreted by the lungs. It also occurs in nature, and leads to formations of stalactites and stalagmites.
The molecular formula for carbonic acid is H2CO3. To find the mass of carbonic acid formed, first calculate the moles of carbon and water. Then, determine the limiting reactant and use it to calculate the moles of carbonic acid formed. Finally, convert the moles of carbonic acid to grams to find the mass.
Carbonic acid can dissolve certain kinds of rock, particularly those that contain calcium carbonate minerals like limestone and marble. The acid reacts with the minerals in the rock, breaking them down and causing them to dissolve over time. This process is known as carbonation weathering.
Carbonic acid is produced by bubbling CO2 into H2O. This reaction forms carbonic acid (H2CO3), which can further dissociate into bicarbonate (HCO3-) and hydrogen ions (H+).